Spec, it looks like some of those pending assays are efforts to tap into the flexure zone as it heads towards 4P and West Winds too?
I haven't come across flexure zones before but I am taking it to mean some kind of cross-cutting channel that runs across the main direction of the fault. Maybe part of the mineralisation seeped laterally into more accommodating rock. Or maybe something happened after the initial mineralisation event that shunted a large zone sideways towards the southeast. Does that sound feasible?
SPR has already noted that mineralisation continues below the flexure so at least it is not a case of bringing a complete halt to discoveries beneath it.
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